利用统计缩尺模式评估阿尔及利亚未来气候预测

Salah Sahabi-Abed
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引用次数: 2

摘要

在本研究中,我们评估了21世纪20年代(2011-2040年)、20世纪50年代(2041-2070年)和20世纪80年代(2071-2100年)三个时期阿尔及利亚的最低温度(T-min)、最高温度(T-max)和降水(PRCP)的未来变化,并以1981-2010年为参考期,重点验证了统计降尺度模型(SDSM)。在这种方法中,为了支持我们的分析,我们通过模拟历史温度和降水来统计地评估SDSM的性能。利用NCEP再分析数据和CanESM2预测因子分别对RCP2.6、RCP4.5和RCP8.5 3种未来情景进行模式定标和未来预测。SDSM应用所产生的气候变化预估结果与先前在阿尔及利亚开展的基于中东-北非地区动态区域气候模式产出的研究结果具有令人信服的一致性。到本世纪末,结果显示,在最坏情况下的极端温度(RCP 8.5)都出现了强烈的变暖,在T-max和阿尔及利亚撒哈拉地区更为明显。在乐观情景下(RCP2.6),对于这两种极端温度,预计变暖的强度都将增加。预估的降水变化揭示了在所有情景下的几个差异,西北地区和撒哈拉中部地区显著减少,而中部和东部沿海地区的预估变化不显著。我们的发现证实了先前使用复杂工具的研究,表明阿尔及利亚的气候预计将在未来进一步变暖。这些初步发现可以概述SDSM统计建模方法在阿尔及利亚等半干旱和干旱脆弱地区的应用,并通过为现有的gcm和区域气候预测提供附加价值,扩展我们在北非地区气候建模领域的知识。此外,关于地方尺度未来变化幅度的可靠信息可用于影响模型,以评估诸如水资源管理、能源和农业等其他关键经济部门变量的变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ASSESSMENT OF FUTURE CLIMATE PROJECTIONS IN ALGERIA USING STATISTICAL DOWNSCALING MODEL
In this study, we assess the future changes in minimum temperature (T-min), maximum temperature (T-max), and precipitation (PRCP) for the three periods the 2020s (2011–2040), the 2050s (2041–2070), and the 2080s (2071–2100), with respect to the reference period 1981–2010 over Algeria focusing on a validation of the Statistical DownScaling Model (SDSM). In this approach, to underpin our analysis, we evaluate statistically the SDSM performance by simulating the historical temperatures and precipitation. The NCEP reanalysis data and CanESM2 predictors of three future scenarios, RCP2.6, RCP4.5, and RCP8.5 are used for model calibration and future projection, respectively. The projected climate changes resulting from the application of SDSM show a convincing consistency with those unveiled in previous studies over Algeria based on dynamical regional climate model outputs conducted in the context of Middle East-North Africa region. By the end of the century, the results exhibit strong warming for both extreme temperatures under the worst-case scenario (RCP 8.5), it is more pronounced for the T-max and over the Algerian Sahara region. Under the optimistic scenario (RCP2.6), the strength of the warming is expected to increase for both extreme temperatures. The projected changes of precipitation revealed for all scenarios several discrepancies with significant decrease over the northwest region and central Sahara, while nonsignificant change is projected for the center and eastern coastal regions. Our findings corroborate previous studies using sophisticated tools by demonstrating that Algeria’s climate is expected to warm further in the future. These primary findings could give an overview of the application of the statistical modeling approach using SDSM over a semi-arid and arid vulnerable region like Algeria and would extend our knowledge in the climate-modelling field for the North Africa zone by providing an added value to the existing GCMs and regional climate projections. In addition, reliable information regarding the magnitude of future changes at local scale may be used in impact models to assess changes of other key economic sector variables such as water resources management, energy and agriculture.
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